4.7 Article

The mineralogy of the CaO-Al2O3-SiO2-H2O(CASH) hydroceramic system from 200 to 350 degrees C

Journal

CEMENT AND CONCRETE RESEARCH
Volume 39, Issue 1, Pages 45-53

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.cemconres.2008.10.002

Keywords

Hydration products; X-ray diffraction; Oil well cement; Geothermal well cement

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We describe a quantitative mineralogical study of the hydrothermal reactions of an oil well cement with added silica and alumina, hydrated at temperatures from 200 to 350 degrees C. We compare the products with pure end member systems and find phase stability can be altered radically, even by small amounts of additive. The upper temperature limits of alpha-C2SH (<250 degrees C), and 1.1 nm tobermorite C5S6H5 (<300 degrees C) are increased. C8S5, reported in a cement-based system for the first time, is stable to 300 degrees C and is believed to prevent foshagite C4S3H formation below 350 degrees C. Hydrogarnet C(3)AS(3-y)H(2y) is the only aluminum bearing phase at <300 degrees C but it coexists with C(4)A(3)H(3) and bicchulite C(8)A(4)Si(4)H(4) at higher temperatures. The presence of alumina increases the stability of 1.1 nm tobermorite greatly and also to a lesser degree of gyrolite. (c) 2008 Elsevier Ltd. All rights reserved.

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